Erinin Martin A, Sagan Cole R, Ahmed Ilian, Pokrifka Gwenore F, Jeevanjee Nadir, Weichman Marissa L, Deike Luc
Department of Mechanical and Aerospace Engineering, Princeton University, Princeton, New Jersey 08540, USA.
Department of Chemistry, Princeton University, Princeton, New Jersey 08540, USA.
Rev Sci Instrum. 2025 May 1;96(5). doi: 10.1063/5.0255658.
We present a new experimental facility to investigate the nucleation and growth of liquid droplets and ice particles under controlled conditions and characterize processes relevant to cloud microphysics: the rapid expansion aerosol chamber (REACh). REACh is an intermediate size chamber (∼0.14 m3) combining the principle of an expansion chamber with the ability to probe the influence of turbulent flows. Water droplet heterogeneous nucleation onto seeding aerosols is achieved via a sudden pressure drop accompanied by a temperature drop, which can cause humid air to condense into a cloud of droplets under appropriate thermodynamic conditions. REACh features tight control and monitoring of the initial saturation ratio of water vapor, identity and concentration of seeding aerosol particles, temperature, pressure, and air flow mixing, together with high speed real-time measurements of aerosol and droplet size and number. Here, we demonstrate that the minimum temperature reached during each expansion can be reasonably described by the thermodynamics of dry or moist adiabats for a range of initial relative humidities. The size and number of droplets formed and the overall lifetime of the cloud are characterized as a function of the aerosol concentration and initial water vapor saturation ratio. The total droplet concentration scales linearly with the seeding aerosol concentration, suggesting that all injected aerosol particles serve as condensation nuclei. While the total number of droplets formed increases with aerosol concentration, the mean droplet size decreases with the concentration of seeding aerosols as a result of competition for the available water vapor. Theoretical considerations provide a quantitative prediction for the mean droplet size over a range of conditions. The high repetition rate of experiments that we can perform with the REACh facility will permit extensive characterization of aerosol processes, including droplet and ice nucleation onset and growth, and the importance of turbulence fluctuations. We will leverage the capabilities of this facility to explore a wide range of physical parameters encompassing regimes relevant to cloud microphysics.
我们展示了一种新的实验装置,用于在可控条件下研究液滴和冰粒子的成核与生长,并表征与云微物理学相关的过程:快速膨胀气溶胶室(REACh)。REACh是一个中等尺寸的室(约0.14立方米),它结合了膨胀室的原理以及探测湍流影响的能力。通过伴随温度下降的突然压降,实现了水滴在种子气溶胶上的异质成核,这在适当的热力学条件下可使潮湿空气凝结成液滴云。REACh的特点是能够严格控制和监测水蒸气的初始饱和比、种子气溶胶粒子的特性和浓度、温度、压力以及气流混合情况,同时还能对气溶胶和液滴的尺寸及数量进行高速实时测量。在此,我们证明,对于一系列初始相对湿度,每次膨胀过程中达到的最低温度可以通过干绝热或湿绝热的热力学合理描述。所形成液滴的尺寸和数量以及云的整体寿命被表征为气溶胶浓度和初始水蒸气饱和比的函数。液滴总浓度与种子气溶胶浓度呈线性比例关系,这表明所有注入的气溶胶粒子都充当了凝结核。虽然形成的液滴总数随气溶胶浓度增加,但由于对可用水蒸气的竞争,平均液滴尺寸随种子气溶胶浓度的增加而减小。理论考量为一系列条件下的平均液滴尺寸提供了定量预测。我们利用REACh装置能够进行的高重复率实验,将对气溶胶过程进行广泛表征,包括液滴和冰的成核起始与生长,以及湍流波动的重要性。我们将利用该装置的能力来探索涵盖与云微物理学相关区域的广泛物理参数。